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In the Southwest, most of our surface water comes from only two river basin
systems—the Colorado River and its tributaries the Rio Grande and its tributaries.
"The Colorado River," said the Bureau of Reclamation in its Internet
site, "is more than 1400 miles in length, making it the third longest river
in the United States. The watershed covers more than 244,000 square miles, 1/12
of the area of the lower 48 states. Although the river begins in the Rocky Mountains,
most of its length drains the arid Southwest region."
Fed primarily by rainwater and snowmelt, the Colorado River rises in north
central Colorado and flows through southeastern Utah and northwestern Arizona
(including the Grand Canyon). It serves as the borders between Nevada and Arizona
and between California and Arizona. It empties into the Gulf of California. Important
tributaries, also fed primarily by rainwater and snowmelt from our mountain ranges,
include the Green River, which rises in western Wyoming; the San Juan River,
in south-central Colorado; the Virgin River, in southwestern Utah; the Little
Colorado River, in east-central Arizona; and the Gila River, in southwestern
Water volumes flowing through the river basin vary widely from year to year,
according to USGS's report "Climatic Fluctuations, Drought, and Flow in
the Colorado River Basin." For instance, from 1983 through 1985, an average
of 20.3 million acre-feet per year flowed through the stream gauging station
at Lee's Ferry, upstream from Grand Canyon and just below the Utah-Arizona border.
From 1933 through 1935, during the punishing Dust Bowl days of the Southern Plains,
an average of 8.0 million acre-feet per year flowed through the station. From
1954 through 1956, another period of severe drought, an average of 7.3 million
acre-feet per year flowed through the station. From 2001 through 2003, an average
of only 5.4 million acre-feet per year – roughly one fourth of the average
for 1983 through 1985 – flowed through the station.
Within the limits imposed by precipitation over time, surplus water can be
banked in good years and drawn down in lean years, thanks to a system of major
dams, canals and aqueducts. Major impoundments include, for instance, Lakes Mojave
and Havasu, on the Arizona/California border; Lake Powell, on the Arizona/Utah
border; and Lake Mead – the largest reservoir in the United States – on
the Arizona/Nevada border.
Importantly, as Noah D. Hall, Bret B. Stuntz, and Robert H. Abrams said in
their paper "Climate Change and Freshwater Resources," Natural Resources & Environment, "The
Colorado River is the only significant water source for much of the Southwest." Altogether
it serves a region of some 25 million people, according to Dan McFadden, MSNBC,
in his article "Colorado River a Strained Lifeline."
At present, drought and global warming are exacting a toll. "Stream
inflows to reservoirs will decline significantly because of diminished snowpack,
reduced soil moisture and increased evaporation before midcentury," said
Hall, Stuntz and Abrams. Snowpack volumes have fallen more than 15 percent since
the middle of the 20th century.
The effects show clearly in the high water marks – or, the "bathtub
rings" – around Colorado River lakes, well above the current water
levels. For instance, although in the early spring of 2008, Lakes Mojave (with
a capacity of 1.8 million acre-feet) and Havasu (with a capacity of 648 thousand
acre-feet) stood at reasonably good shape – each about 80 to 90 percent
full – the much larger Lakes Powell (capacity 24 million acre-feet) and
Mead (capacity 28 million acre-feet) had dwindled to roughly 50 percent full.
While Southern California alone expects its water demand to grow by 37 percent
by 2020 according to McFadden, agricultural, municipal, industrial and domestic
users are already consuming every drop of surface water available in the basin.
Indeed, Colorado River waters have not reached the Gulf of California for years.
The second major source of surface water, the Rio Grande, runs for roughly
1850 miles from its 12,000-foot high source, in the San Juan and Sangre de Cristo
Mountains of southwestern Colorado, to the Gulf of Mexico, at the southernmost
tip of Texas. Its watershed encompasses more than 300,000 square miles in the
United States and Mexico, although only about half that arid region actually
contributes water to the river, said the Encyclopaedia Britinnica.
Fed primarily, like the Colorado River, by rainwater and snowmelt, the Rio
Grande courses down the steep mountain slopes of Colorado, runs southward through
New Mexico's heart, turns southeastward at El Paso/Juarez, describes the great
arc of the Big Bend, then flows southeastward to the Gulf. From El Paso/Juarez
to Brownsville, a distance of more than 1000 miles, the river defines the border
between the United States and Mexico, dividing the state of Texas from the Mexican
states of Chihuahua, Coahuila, Nuevo Leon and Tamaulipas. "Many of the
river tributaries are intermittent streams," said USGS in "Monitoring
the Water Quality of the Nation's Large Rivers," published in its Science
for a Changing World Internet site. "Much of the flow is controlled by
numerous reservoirs in the basin. Throughout the basin, an extensive system of
water structures captures and controls the flow of water in the subbasins to
meet regional needs for flood control, power generation, and storage for domestic,
agricultural, and industrial purposes." Important impoundments include
the Elephant Butte Reservoir, with a capacity of about two million acre feet,
and the Caballo Reservoir, with a capacity of about 226 thousand acre feet—about
the same capacity as Lakes Mojave and Havasu combined. According to Bureau of
Reclamation data, Elephant Butte will only be about half full and Caballo, about
one fourth full, even following the well-above-average snowmelt expected for
the spring of 2008.
Overall, the Rio Grande carries far less water than the Colorado River. It
may receive several hundred thousand acre feet of water from melting 50-foot
high snow deposits near the peaks of the mountains in the spring, according to
the Colorado State University Internet site. It receives varying amounts of waters
from the Chama River in northern New Mexico, the intermittent Puerco River in
central New Mexico, the Pecos River and Devils River below Big Bend, Mexico's
Concho River just west of Big Bend and Mexico's Salado River some 150 miles upstream
from the Gulf of Mexico. It serves a region with more than some 13 million U.
S. and Mexican people, according to the NBC Weather Internet site (including
nearly three million in the El Paso/Juarez area alone).
In recent years, the surface waters that the Rio Grande receives from the
Colorado Mountains and New Mexico tributaries have been completely exhausted
by the time the river reaches Fort Quitman, about 40 miles downstream from the
El Paso/Juarez region. It frequently runs as no more than a dry stream bed through
the Chihuahuan Desert for the next 150 miles, until it reaches the border cities
of Presidio and Ojinaga, where Mexico's Concho River brings new life to the Rio
Grande. The segment of the river from Colorado to Fort Quitman is often called
the Upper Rio Grande Basin. The segment from Fort Quitman to the Gulf of Mexico
is called the Lower Rio Grande Basin. In effect, the historic Rio Grande, serving
an area with rapidly increasing population and growing demands, now functions
as two separate rivers. "The once-mighty Rio Grande is so tapped out it
doesn't even reach the Gulf of Mexico anymore," according to the U. S. Water
News Online, August 2001.
Increase in the demand for water across the Southwest mirrors the growth
of population. Exemplifying the trends, total consumption just in the southeastern
counties of California and in the states of Arizona and New Mexico increased
by nearly nine percent just from 1985 to 2000, or from about 13.47 million acre
feet to about 14.63 million acre feet during the 15-year period. Some 30 to 40
percent was withdrawn from ground waters and the balance, from surface waters,
according to data from Konieczki's and Heilman's Water-Use Trends in the Desert
Southwest—1950 – 2000.
While some 80 to 90 percent of the water was allocated to agricultural uses,
an increasing percentage was directed to domestic consumption—an indication
that, as Konieczki and Heilman said, "The population in the Desert Southwest
is among the fastest growing in the country."
Concurrently, in Mexico's part of the Rio Grande Basin, water demands and
population continue to grow. For instance, even though the city's aquifer – the
Hueco Bolson – is dwindling rapidly, tens of thousands of Mexican citizens
continue to pour into Juarez, across the Rio Grande from El Paso, every year.
The estimated population of the city now approaches two million, which is about
equal to the population of the entire state of New Mexico.
The combination of growing demand and shrinking water resources across the
Southwestern United States and northeastern Mexico have raised a galaxy of physical,
social and political problems, which we will address in Part II of "Dust
Bowl in the Southwest?"
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